Instrumental records do not go back far enough to provide us with reliable measurements of global climatic variability on timescales longer than a century.
仪器上记录的年代不够久远，因而无法可靠地提供一个世纪以前全球气候变化的测量值。
The climatic models simulated by proxy indices reflecting solar activity point out that solar variability can interpret most of temperature change before 1850.
根据多种反映太阳活动的代用指标拟合的气候模型指出，太阳活动可以解释1850年以前气温变化的大部分情况。
Zhou Liantong, Huang Ronghui. 2006. Characteristics of interdecadal variability of spring precipitation in North China and its possible cause [J]. Climatic Environ Res, 11 (4) : 441-450.
周连童，黄荣辉。2006。我国华北地区春季降水的年代际变化特征及其可能成因的探讨[j]。气候与环境研究，11 (4)：441 - 450。
Zhou Liantong, Huang Ronghui. 2006. Characteristics of interdecadal variability of spring precipitation in North China and its possible cause [J]. Climatic Environ Res, 11 (4) : 441-450.
周连童，黄荣辉。2006。我国华北地区春季降水的年代际变化特征及其可能成因的探讨[j]。气候与环境研究，11 (4)：441 - 450。
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